Variability of the nutrient stream near Kuroshio's origin

Abstract The Kuroshio—literally “the Black Stream”—is the most substantial current in the Pacific Ocean. It was called the Black Stream because this oligotrophic current is so nutrient-poor in its euphotic zone that the water appears black without the influence of phytoplankton and the associated, o...

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Published in:Scientific Reports
Main Authors: Chen, Chen-Tung Arthur, Huang, Ting-Hsuan, Wu, Chi-Hsuan, Yang, Haiyan, Guo, Xinyu
Other Authors: Ministry of Education, Ministry of Science and Technology, Taiwan
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2021
Subjects:
Online Access:http://dx.doi.org/10.1038/s41598-021-84420-5
http://www.nature.com/articles/s41598-021-84420-5.pdf
http://www.nature.com/articles/s41598-021-84420-5
id crspringernat:10.1038/s41598-021-84420-5
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spelling crspringernat:10.1038/s41598-021-84420-5 2023-05-15T18:28:29+02:00 Variability of the nutrient stream near Kuroshio's origin Chen, Chen-Tung Arthur Huang, Ting-Hsuan Wu, Chi-Hsuan Yang, Haiyan Guo, Xinyu Ministry of Education Ministry of Science and Technology, Taiwan 2021 http://dx.doi.org/10.1038/s41598-021-84420-5 http://www.nature.com/articles/s41598-021-84420-5.pdf http://www.nature.com/articles/s41598-021-84420-5 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Scientific Reports volume 11, issue 1 ISSN 2045-2322 Multidisciplinary journal-article 2021 crspringernat https://doi.org/10.1038/s41598-021-84420-5 2021-11-02T17:21:32Z Abstract The Kuroshio—literally “the Black Stream”—is the most substantial current in the Pacific Ocean. It was called the Black Stream because this oligotrophic current is so nutrient-poor in its euphotic zone that the water appears black without the influence of phytoplankton and the associated, often colored dissolved organic matter. Yet, below the euphotic layer, nutrient concentrations increase with depth while current speed declines. Consequently, a core of maximum nutrient flux, the so-called nutrient stream, develops at a depth of roughly between 200 and 800 m. This poorly studied nutrient stream transports nutrients to and supports high productivity and fisheries on the East China Sea continental shelf; it also transports nutrients to and promotes increased productivity and fisheries in the Kuroshio Extension and the subarctic Pacific Ocean. Three modes of the Kuroshio nutrient stream are detected off SE Taiwan for the first time: one has a single-core; one has two cores that are apparently separated by the ridge at 120.6–122° E, and one has two cores that are separated by a southward flow above the ridge. More importantly, northward nutrient transports seem to have been increasing since 2015 as a result of a 30% increase in subsurface water transport, which began in 2013. Such a nutrient stream supports the Kuroshio's high productivity, such as on the East China Sea continental shelf and in the Kuroshio Extension SE of Japan. Article in Journal/Newspaper Subarctic Springer Nature (via Crossref) Pacific Scientific Reports 11 1
institution Open Polar
collection Springer Nature (via Crossref)
op_collection_id crspringernat
language English
topic Multidisciplinary
spellingShingle Multidisciplinary
Chen, Chen-Tung Arthur
Huang, Ting-Hsuan
Wu, Chi-Hsuan
Yang, Haiyan
Guo, Xinyu
Variability of the nutrient stream near Kuroshio's origin
topic_facet Multidisciplinary
description Abstract The Kuroshio—literally “the Black Stream”—is the most substantial current in the Pacific Ocean. It was called the Black Stream because this oligotrophic current is so nutrient-poor in its euphotic zone that the water appears black without the influence of phytoplankton and the associated, often colored dissolved organic matter. Yet, below the euphotic layer, nutrient concentrations increase with depth while current speed declines. Consequently, a core of maximum nutrient flux, the so-called nutrient stream, develops at a depth of roughly between 200 and 800 m. This poorly studied nutrient stream transports nutrients to and supports high productivity and fisheries on the East China Sea continental shelf; it also transports nutrients to and promotes increased productivity and fisheries in the Kuroshio Extension and the subarctic Pacific Ocean. Three modes of the Kuroshio nutrient stream are detected off SE Taiwan for the first time: one has a single-core; one has two cores that are apparently separated by the ridge at 120.6–122° E, and one has two cores that are separated by a southward flow above the ridge. More importantly, northward nutrient transports seem to have been increasing since 2015 as a result of a 30% increase in subsurface water transport, which began in 2013. Such a nutrient stream supports the Kuroshio's high productivity, such as on the East China Sea continental shelf and in the Kuroshio Extension SE of Japan.
author2 Ministry of Education
Ministry of Science and Technology, Taiwan
format Article in Journal/Newspaper
author Chen, Chen-Tung Arthur
Huang, Ting-Hsuan
Wu, Chi-Hsuan
Yang, Haiyan
Guo, Xinyu
author_facet Chen, Chen-Tung Arthur
Huang, Ting-Hsuan
Wu, Chi-Hsuan
Yang, Haiyan
Guo, Xinyu
author_sort Chen, Chen-Tung Arthur
title Variability of the nutrient stream near Kuroshio's origin
title_short Variability of the nutrient stream near Kuroshio's origin
title_full Variability of the nutrient stream near Kuroshio's origin
title_fullStr Variability of the nutrient stream near Kuroshio's origin
title_full_unstemmed Variability of the nutrient stream near Kuroshio's origin
title_sort variability of the nutrient stream near kuroshio's origin
publisher Springer Science and Business Media LLC
publishDate 2021
url http://dx.doi.org/10.1038/s41598-021-84420-5
http://www.nature.com/articles/s41598-021-84420-5.pdf
http://www.nature.com/articles/s41598-021-84420-5
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_source Scientific Reports
volume 11, issue 1
ISSN 2045-2322
op_rights https://creativecommons.org/licenses/by/4.0
https://creativecommons.org/licenses/by/4.0
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